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    Experimental Observations of Flow and Bed Processes in Large-Amplitude Meandering Flume

    Source: Journal of Hydraulic Engineering:;2009:;Volume ( 135 ):;issue: 007
    Author:
    Donatella Termini
    DOI: 10.1061/(ASCE)HY.1943-7900.0000046
    Publisher: American Society of Civil Engineers
    Abstract: Meanders of large amplitude often exhibit asymmetric planform shape or subsidiary bends. The present work is aimed at improving on understanding of the morphodynamic phenomena affecting the bed evolution of large amplitude meandering channels. Attention is focused on the development of the steady point bar-pool configuration and of the superimposed large-scale migrating bed forms; of particular interest is the role of the changing channel curvature and bed topography variation on flow pattern. A series of experiments was carried out in a sine-generated large-amplitude meandering flume, for two values of width-to-depth ratio. Maps documenting the bed topography and the flow pattern along the meandering bends are reported. Two point bars per bend were observed and seem to be part of a series of damped oscillations developing in response to the changing channel curvature. In response to the bed deformation, the maximum flow velocity moves at the outer bank at the entrance of the bend.
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      Experimental Observations of Flow and Bed Processes in Large-Amplitude Meandering Flume

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    contributor authorDonatella Termini
    date accessioned2017-05-08T21:50:33Z
    date available2017-05-08T21:50:33Z
    date copyrightJuly 2009
    date issued2009
    identifier other%28asce%29hy%2E1943-7900%2E0000083.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/63882
    description abstractMeanders of large amplitude often exhibit asymmetric planform shape or subsidiary bends. The present work is aimed at improving on understanding of the morphodynamic phenomena affecting the bed evolution of large amplitude meandering channels. Attention is focused on the development of the steady point bar-pool configuration and of the superimposed large-scale migrating bed forms; of particular interest is the role of the changing channel curvature and bed topography variation on flow pattern. A series of experiments was carried out in a sine-generated large-amplitude meandering flume, for two values of width-to-depth ratio. Maps documenting the bed topography and the flow pattern along the meandering bends are reported. Two point bars per bend were observed and seem to be part of a series of damped oscillations developing in response to the changing channel curvature. In response to the bed deformation, the maximum flow velocity moves at the outer bank at the entrance of the bend.
    publisherAmerican Society of Civil Engineers
    titleExperimental Observations of Flow and Bed Processes in Large-Amplitude Meandering Flume
    typeJournal Paper
    journal volume135
    journal issue7
    journal titleJournal of Hydraulic Engineering
    identifier doi10.1061/(ASCE)HY.1943-7900.0000046
    treeJournal of Hydraulic Engineering:;2009:;Volume ( 135 ):;issue: 007
    contenttypeFulltext
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